Gao G.F., Li P.F., Zhong J.X., Shen Z.J., Chen J., Li Y.T., Isabwe A., Zhu X.Y., Ding Q.S., Zhang S., Gao C.H. and Zheng H.L.. 2019. Science of the Total Environment, 653: 231-240.
Chinese mangrove, an important ecosystem in coastal wetlands, is sensitive to the invasive alien species Spartina alterniflora. However, the effects of the S. alterniflora invasion on mangrove soil N2O emissions and the underlying mechanisms by which emissions are affected have not been well studied. In this study, the N2O emitted from soils dominated by two typical native mangroves (i.e. Kandelia obovata: KO; Avicennia marina: AM), one invaded by S. alterniflora (SA), and one bare mudflat (Mud) were monitored at Zhangjiang Mangrove Estuary (where S. alterniflora is exotic). Together with soil biogeochemical properties, the potential denitrification rate and the composition of soil bacterial communities were determined simultaneously by 15NO3− tracer and high-throughput sequencing techniques, respectively. Our results showed that S. alterniflora invasion significantly (p＜0.05) increases soil N2O emissions by 15–28-fold. In addition, isotope results revealed that the soil potential denitrification rate was significantly (p＜0.05) enhanced after S. alterniflora invasion. Moreover, the S. alterniflora invasion significantly (p＜0.05) decreased soil bacterial α-diversity and strongly modified soil bacterial communities. Indicator groups strongly associated with S. alterniflora were Chloroflexia, Alphaproteobacteria, and Bacilli, each of which was abundant and acts as connector in the co-occurrence network. FAPROTAX analysis implied that the S. alterniflora invasion stimulated soil denitrification and nitrification while depressing anaerobic ammonium oxidation (anammox) and dissimilatory nitrate reduction to ammonium (DNRA). Redundancy analysis (RDA) found that soil organic matter (SOM) and pH were the most important environmental factors in altering soil bacterial communities. Taken together, our results imply that the S. alterniflora invasion in mangrove wetlands significantly stimulates soil denitrification and N2O emissions, thereby contributing N2O to the atmosphere and contributing to global climate change.
Figure 1. Differences in soil bacterial communities among sites. Relative abundance of the top 10 phyla (a); Venn plot at genus level (b); hierarchical clustering tree on OTU level using Weighted-UniFrac distance (c); non-metric multi-dimensional scaling (NMDS) on OTU level using Bray-Curtis distance (d). KO: K. obovata; AM: A. marina; SA: S. alterniflora; Mud: bare mudflat.
